kappakertymän
Kappakertymän refers to a specific type of geological formation found in Finland. It is characterized by accumulations of sorted sand and gravel, often deposited by flowing water during glacial periods. These formations are typically found in eskers, which are long, winding ridges formed by meltwater streams beneath glaciers.
The composition of kappakertymän varies, but it generally consists of sand grains, pebbles, and cobbles. The
Kappakertymän formations are important for understanding past glacial dynamics and the paleoenvironment of Finland. They can